PLATE TECTONICS
- History of Plate Tectonics and Continental Drift
- Abraham Ortelius (1596 ) - continents fit like jigsaw puzzle
- Edward Suess (1855)
- noted that Late Paleozoic plant fossils in India, Australia, Africa, Antarctica, and South America all look the
same
- Gondwanaland
- Antonio Snider-Perlligrini (1858)
- wrote Creation and its mysteries revealed and showed (with maps) how the continents looked before they
separated
- sited fossil evidence (North America and Europe)
- attributed the separation of the continents to the biblical deluge
- Frank B. Taylor (1908)
- pointed out that several geologic facts could be explained by continental drift
- suggested that the Mid-Atlantic Ridge marked the site along which an ancient continent broke apart to form
the present-day Atlantic Ocean
- Alfred Wegner (1915)
- considered the father of Continental Drift
- wrote "The origin of the continents and oceans"
- drew series of maps that showed 3 stages of continental drift
- began with Pangea ("all land")
- believed that the continents (composed of light granitic rock) plowed through the denser rocks of the ocean
floor
- driven by forces related to the rotation of the earth
- Arthur Holmes (1928) - provided a mechanism
- Thermal convection in the mantle
- Alexander du Toit (1937)
- wrote "Our wondering continents"
- noted climatological paradox of where coal beds and glacial deposits are today
- solved by moving Pangea to the south pole and North America to the equator and called the new landmass
Laurasia
- Harry Hess (1960's)
- given credit for thermal convection along mid ocean ridges
- Early Evidence for Continental Drift
- continental fit
- rock sequences
- glacial evidence
- fossil evidence
- polar wandering
- Recent Evidence for Continental Drift
- seafloor spreading - 1960's
- deep-sea drilling
- magnetic anomalies
- age dating of rock
- Modern Plate Tectonics Theory
- the lithosphere is divided into plates, bounded by oceanic ridges, trenches, mountain ranges, and transform faults
- Types of Boundaries and features
- Divergent Plate Boundaries
- seafloor plate separation
- continental plate separation
- Convergent Plate Boundaries
- island arcs
- deep sea trenches
- Transform Boundaries
- Combinations
- Rates of Plate Motion
- paleomagnetics and anomalies
- magma generated at MOR become magnetized to the current orientation of the poles
- deep-sea drilling
- provided sediments from the ocean floors, some of which could be age dated either with fossils or with
radiometric dating
- isochrons
- contours of equal time showing how much time has elapsed since the oceanic crustal rocks were first
formed
- Geometry of Plate Motion
- transform boundaries
- indicates the direction of plate motion
- isochrons
- indicates the position of plates at past times
- satellite measurements of plate motions